Kootenay Boundary

We're into a period of HIGH danger with rapid loading of the snowpack on Wednesday into Thursday: rain to treeline and heavy snow in the alpine.

Moderate - Intensity of incoming weather systems is uncertain

Warm and wet on Wednesday through Thursday. Cooling with isolated flurries on Friday, and Saturday. THURSDAY: Rain or wet snow (20-30 mm / cm) Wednesday overnight and another 20-30 mm / cm during the day Thursday. / Moderate southerly winds / Freezing level around 1600 m. FRIDAY: Mostly cloudy with lisolated flurries possible (5-10cm) / High temperatures to -1 Celsius / Light westerly winds / Freezing level around 1300 m. SATURDAY: Cloudy with light snow (5-15cm) / Ridge winds light southerly / Freezing level around 1100m / High temperatures to -2 Celsius.

In the Rossland Range deep persistent slabs to Size 2 were reported on southeast and west aspects around 2000m. A thin snowpack or solar triggered sluffs stepping down to weaker faceted layers were the culprits. Of particular note was a Size 3 natural avalanche on Wolf ridge near Kootenay pass on Monday - the sun's effect is significant! See the great photo in the MIN report (here).

The recent warming and sunny conditions gave us a widespread sun crust on all but high northerly (and some westerly) aspects, where there is still some cold snow to be found. These will be excellent sliding surfaces for incoming new snow.At the end of last week up to 30cm additional snow fell (mostly near Nelson) and brought the recent storm snow total to 65-100cm, creating touchy storm slabs at all upper elevations and aspects. Slabs were reported as very reactive to human triggers and are sitting on a variety of surfaces; including scoured surfaces in wind exposed terrain, surface hoar (size 2-3 mm) in sheltered locations, and sun crust on steep solar aspects.Snowpack tests near the Valhallas have given moderate, propagation-likely results down 50-70cms on the Feb 3rd interface. Areas with a shallower snowpack (less than 150 cm) have a generally weak snowpack structure with sugary facets near the ground. This includes shallow alpine slopes and most of the Rossland range. It is possible for storm slab avalanches to step-down to these deeper weak layers, resulting in large, destructive avalanches.